第8层古土壤特殊的厚层淀积代表了气候的多次变化和多个成壤期。
The thick illuvial horizon in the 8th paleosol layer indicates the repeated soil-forming processes and climate changes.
三个土壤剖面均有一定的漂洗和淀积粘化现象，但都不足以定义成漂白层或粘盘层。
Bleaching and characterization were morphologically apparent, but not well developed as to be defined as bleached or claying horizons.
三个土壤剖面均有一定的漂洗和淀积粘化现象，但都不足以定义成漂白层或粘盘层。
Bleaching and characterization were morphologically apparent, but not well developed as to be defined as bleached or claying horizons.
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